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Journal articles on the topic 'Teisseire'

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Published: 4 June 2021

Last updated: 17 February 2022

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1

Hayez, Anne-Marie. "Le patrimoine urbain d’un marchand cordier avignonnais : Jean Teisseire († 1384)." Bibliothèque de l'école des chartes 154, no. 2 (1996): 427–84. http://dx.doi.org/10.3406/bec.1996.450827.

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2

de Amorim, Renato Cordeiro. "Pascal Poncelet, Florent Masseglia, Maguelonne Teisseire: Successes and New Directions in Data Mining." Information Retrieval 12, no. 4 (September 12, 2008): 504–8. http://dx.doi.org/10.1007/s10791-008-9068-6.

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3

Dubois-Morestin, Mélanie. "Techniques, usages et commercialisation du chanvre à travers les archives privées d’un cordier du xive siècle, Jean Teisseire." Annales de Bretagne et des pays de l'Ouest, no. 127 (October 8, 2020): 21–32. http://dx.doi.org/10.4000/abpo.6236.

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4

Dubois, Mélanie. "Écrits et pratiques du crédit au xive siècle à Avignon à travers les archives privées d'un marchand cordier, Jean Teisseire." Hypothèses 16, no. 1 (2013): 105. http://dx.doi.org/10.3917/hyp.121.0105.

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5

Fischer, Nikolaus H. "Chemistry of Fragrant Substances Paul Jose Teisseire. VCH Publishers, Inc., New York, NY. 1994. vi + 458 pp. 155 × 23.5 cm. $125.00. ISBN 1-56081-610-4." Journal of Natural Products 59, no. 12 (January 1996): 1212. http://dx.doi.org/10.1021/np960319q.

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6

Sroka, Stanisław Tadeusz. "The Contribution of the Teisseyre Family to Polish Culture." Perspektywy Kultury 30, no. 3 (December 20, 2020): 271–88. http://dx.doi.org/10.35765/pk.2020.3003.18.

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The article discusses the role of members of the Teisseyre family in contributing to Polish culture. The Teisseyre family, originally from France, settled in Poland after the French Revolution and quickly became Polonized. Subsequent generations made a significant contribution to the cultural development of our country. They marked their presence primarily in the hard sciences (Wawrzyniec, Henryk, Juliusz, Andrzej, Mieczysław, and Roman Teisseyre), but also in the fields of technology (Jerzy and Andrzej Teisseyre) and art (Stanisław Teisseyre). Modern descendants who are active in various fields of culture try to continue the family traditions.

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7

Könst, W. M. B. "Chemistry of Fragrant Substances P.J. Teisseire VCH, Weinheim, 1994 vi + 458 pages. DM 218.00 / £ 89.00 ISBN 1-56081-610-4 Publishers, Inc. ISBN 3-527-89610-4 VCH Verlagsgesellschaft." Recueil des Travaux Chimiques des Pays-Bas 113, no. 7-8 (1994): 381. http://dx.doi.org/10.1002/recl.19941130712.

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8

Coquery, Natacha. "Hommage à Line Teisseyre-Sallmann." Histoire urbaine 31, no. 2 (2011): 181. http://dx.doi.org/10.3917/rhu.031.0181.

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9

Mazur, Stanisław, Piotr Krzywiec, Michał Malinowski, Marek Lewandowski, Paweł Aleksandrowski, and Mateusz Mikołajczak. "On the nature of the Teisseyre-Tornquist Zone." Geology, Geophysics & Environment 44, no. 1 (2018): 17. http://dx.doi.org/10.7494/geol.2018.44.1.17.

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10

KRÓLIKOWSKI, C., and Z. PETECKI. "Crustal structure at the Trans-European Suture Zone in northwest Poland based on gravity data." Geological Magazine 134, no. 5 (September 1997): 661–67. http://dx.doi.org/10.1017/s0016756897007395.

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A new gravity model of the crustal structure of the Trans-European Suture Zone in the northwestern Poland has been constructed. The Bouguer anomaly map, obtained after stripping off the three-dimensional gravity effect of the sedimentary cover down to the Zechstein formations, is characterized by a 50 mGal gravity anomaly. We have assumed that the short-wavelength components derive from upper crustal intrusions and the long-wavelength components reflect crustal thickness and lateral heterogeneity which are strongly supported by the new seismic data along the LT-7 geotraverse. Quantitative modelling of gravity data along three profiles crossing the area indicate the presence of anomalous masses within the Lower Palaeozoic sequence, mainly along the Teisseyre-Tornquist Zone. Two of the profiles crossing the long-wavelength ‘stripped’ gravity high suggest the existence of a zone of 35 km crust above a dense upper mantle along the Teisseyre-Tornquist Zone. The extent of the zone can be determined based on the Bouguer anomalies interpretation.

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11

Schweitzer, Johannes. "Blockage of regional seismic waves by the Teisseyre-Tornquist zone." Geophysical Journal International 123, no. 1 (October 1995): 260–76. http://dx.doi.org/10.1111/j.1365-246x.1995.tb06674.x.

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12

THYBO, HANS. "Geophysical characteristics of the Tornquist Fan area, northwest Trans-European Suture Zone: indication of late Carboniferous to early Permian dextral transtension." Geological Magazine 134, no. 5 (September 1997): 597–606. http://dx.doi.org/10.1017/s0016756897007267.

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The Tornquist Fan is a northwestward widening splay of late Carboniferous–early Permian fault zones in the region of Denmark emanating from the Teisseyre-Tornquist Zone in northern Poland. The crust–mantle boundary shows an undulating topography which correlates with the main tectonic features of the area. Zones of high average velocity through the consolidated crust coincide with pronounced positive Bouguer gravity anomalies in the deep basins and in the border zone of the shield. Less pronounced, similar correlation to gravity is found for the thickness of the lower crust, whereas the thickness of the upper crust in parts is inversely related to the gravity anomalies. Some magnetic anomalies appear to be related to the gravity anomalies. The positive features are interpreted as magmatic bodies that formed during late Carboniferous to early Permian transtensional movement along the faults of the Tornquist Fan, which explains pull-apart structures in the area and the Ringkøbing-Fyn basement High. The magmatism has strong implications for the subsequent formation of the regional Mesozoic basins. Localized dextral strike-slip movement on the Teisseyre-Tornquist Zone became distributed over the Tornquist Fan, which formed part of the rigid Baltic Shield and was situated at the northwestern end of this major, long-reaching Central European zone. As defined by late Cretaceous–early Tertiary compressional inversion structures, the Sorgenfrei-Tornquist Zone cuts across the Tornquist Fan area.

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13

Konon, Andrzej, Szymon Ostrowski, Barbara Rybak-Ostrowska, Mirosław Ludwiniak, Michał Śmigielski, Michał Wyglądała, Joanna Uroda, Sebastian Kowalczyk, Radosław Mieszkowski, and Agnieszka Kłopotowska. "Mnin restraining stepover – evidence of significant Cretaceous–Cenozoic dextral strike-slip faulting along the Teisseyre-Tornquist Zone?" Acta Geologica Polonica 66, no. 3 (September 1, 2016): 435–55. http://dx.doi.org/10.1515/agp-2016-0019.

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Abstract A newly recognized Mnin restraining stepover is identified in the Permo-Mesozoic cover of the western part of the Late Palaeozoic Holy Cross Mountains Fold Belt (Poland), within a fault pattern consisting of dextral strike-slip faults. The formation of a large contractional structure at the Late Cretaceous – Cenozoic transition displays the significant role of strike-slip faulting along the western border of the Teisseyre-Tornquist Zone, in the foreland of the Polish part of the Carpathian Orogen. Theoretical relationships between the maximum fault offsets/ mean step length, as well as between the maximum fault offsets/mean step width allowed the estimation of the values of possible offsets along the Snochowice and Mieczyn faults forming the Mnin stepover. The estimated values suggest displacements of as much as several tens of kilometres. The observed offset along the Tokarnia Fault and theoretical calculations suggest that the strike-slip faults west of the Late Palaeozoic Holy Cross Mountains Fold Belt belong to a large strike-slip fault system. We postulate that the observed significant refraction of the faults forming the anastomosing fault pattern is related also to the interaction of the NW-SE-striking faults formed along the western border of the Teisseyre- Tornquist Zone and the reactivated WNW-ESE-striking faults belonging to the fault systems of the northern margin of the Tethys Ocean.

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14

Mazur, Stanislaw, Mateusz Mikolajczak, Piotr Krzywiec, Michal Malinowski, Vinton Buffenmyer, and Marek Lewandowski. "Is the Teisseyre‐Tornquist Zone an ancient plate boundary of Baltica?" Tectonics 34, no. 12 (December 2015): 2465–77. http://dx.doi.org/10.1002/2015tc003934.

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15

Gainot, Bernard. "GRANDJEAN, lieutenant LAVAL, Journaux sur l'Expédition d'Égypte, Paris, Librairie historique Teissedre, 2000, 213 p." Annales historiques de la Révolution française, no. 329 (September 1, 2002): 218. http://dx.doi.org/10.4000/ahrf.1264.

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16

Grad, M., T. Janik, J. Yliniemi, A. Guterch, U. Luosto, T. Tiira, K. Komminaho, et al. "Crustal structure of the Mid-Polish Trough beneath the Teisseyre–Tornquist Zone seismic profile." Tectonophysics 314, no. 1-3 (December 1999): 145–60. http://dx.doi.org/10.1016/s0040-1951(99)00241-3.

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17

Alsina, Dolors, and Rod Snieder. "Constraints on the velocity structure beneath the Tornquist-Teisseyre Zone from beam-forming analysis." Geophysical Journal International 126, no. 1 (July 1996): 205–18. http://dx.doi.org/10.1111/j.1365-246x.1996.tb05279.x.

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18

Čermák, Vladimír, Jan Šafanda, and Alexandr Guterch. "Deep temperature distribution along three profiles crossing the Teisseyre-Tornquist tectonic zone in Poland." Tectonophysics 164, no. 2-4 (August 1989): 151–63. http://dx.doi.org/10.1016/0040-1951(89)90009-7.

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19

Mysak, M. "Historical analysis of the hypotheses of tectonic morphogenesis of the Male Polissia Basin." Physical Geography and Geomorphology 89, no. 1 (2018): 16–22. http://dx.doi.org/10.17721/phgg.2018.1.02.

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The hypotheses of morphogenesis of the Male Polissia Basin, where the influence of the tectonic factor is considered, are analyzed in this article. The analysis was carried out on the basis of existing literary and cartographic sources related to geological and geomorphological studies of Male Polissia. Two groups of tectonic hypotheses of morphogenesis of Male Polissia are defined: denudation-tectonic and tectonic-denudation. Suppoters of the denudation-tectonic hypothesis claimed that the main factor in the morphogenesis of the Male Polissia was denudation, and tectonic processes only contributed to increasing its intensity. The representatives of this hypothesis were E. Titze, J. Novak, A. Zierhoffer and J. Czyżewski,H. Zilber, P. Tsis` and I. Chervanov. Most of them, believed that the reason for intense denudation were block tectonic elevations. Their views differed in main intensity and localization of elevations within the Male Polissya and adjacent territories of the Podolian and Volyn’ Uplands, and also Roztochia. Supporters of tectonic-denudation hypotheses considered tectonics as a decisive factor in the morphogenesis of the Male Polissia Basin. In their hypotheses, the main tectonic processes were linear tectonic elevations along the Podolian escarpment, or block tectonic subsidence of the Male Polissia Basin, which, mainly, formed the modern limits of it. Supporters of the tectonic-denudation hypothesis were W. Teisseyre, W. Lozinski, J. Siemiradzki, J. Smolenski, T. Wiśniowski, S. Rudnytskyi, H. Teisseyre, K. Gerenchuk, I. Hofshtein and Y. Swynko. The comparative table of the ideas of researchers regarding the localization and age of tectonic processes, that influenced the genesis of the Male Polissia Basin, is also presented in the work. The existing scientific data on the neotectonic movements of the research area is also analyzed. Data on the intensity, localization and direction of these movements are distinctive. Also, a historical analysis of ideas concerning the tectonic origin of the Hriadove Pobuzhia Upland and the research of stratigraphy of Cretaceous deposits along the border of Male Polissia and Podolian escarpment was carried out.

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20

Wojas, Anna, Teresa Grabowska, and Mateusz Mikołajczak. "Relative secular variations of the geomagnetic field along the Zgorzelec-Wiżajny profile, Poland." E3S Web of Conferences 35 (2018): 03001. http://dx.doi.org/10.1051/e3sconf/20183503001.

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The paper presents results of the study on relative secular variations of total magnetic intensity (TMI) of the geomagnetic field along the 700 km long profile crossing the area of Poland. Surveys were carried out at annual intervals between 1966 and 2016 (50 measurement series), in 31 survey sites (secular points) separated by about 22 km. The studied profile of the SW-NE direction, called Zgorzelec-Wiżajny (Z-W), crosses large parts of the main tectonic units of Europe, namely the Palaeozoic Platform of Central and Western Europe (PLZ) and the East European Craton (EEC), connected by the Teisseyre-Tornquist Zone (TTZ). Using the original methodology of analysis of measured data, reduced to the values of geomagnetic field recorded at the Central Geophysical Observatory in Belsk, the relative secular variations of TMI with the magnetic anomalies (ΔT) and the terrestrial heat flow density (Q) were graphically presented.

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21

Thybo, Hans. "Crustal structure and tectonic evolution of the Tornquist Fan region as revealed by geophysical methods." Bulletin of the Geological Society of Denmark 46 (May 3, 1999): 145–60. http://dx.doi.org/10.37570/bgsd-1999-46-12.

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Crustal structure derived primarily from geophysical investigations reveals features that may be related to the complex tectonic evolution of the Tornquist Fan region. This northwestwards widening splay of Late Carboniferous – Early Permian fault zones in the Danish region emanates from the Teisseyre-Tornquist Zone in northern Poland. Seismic reflections and velocity anomalies image collisional fault zones that formed during the Proterozoic and Palaeozoic amalgamation of the crust. Re-equilibration of Moho appears to have taken place before late Palaeozoic rifting and magmatism initiated the main phase of basin formation that continued into the Mesozoic. The resulting, strong Moho topography, with variation between depths of 26 and 48 km, has been practically “frozen in” since then, although the late Cretaceous – early Cenozoic inversion tectonics may have formed a crustal keel underneath part of the Sorgenfrei-Tornquist Zone which cuts across the Proterozoic crust of the Tornquist Fan region.

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22

Podhalańska, Teresa. "Ichnofossils from the Ordovician mudrocks of the Pomeranian part of the Teisseyre–Tornquist Zone (NW Poland)." Palaeogeography, Palaeoclimatology, Palaeoecology 245, no. 1-2 (March 2007): 295–305. http://dx.doi.org/10.1016/j.palaeo.2006.06.002.

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23

Grad, Marek. "Podolian, Saxonian and baltic plates – Teisseyre–Tornquist Line and the edge of the East European Craton." Geochemistry 79, no. 3 (September 2019): 422–33. http://dx.doi.org/10.1016/j.chemer.2019.03.002.

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24

Środoń, J., and N. Clauer. "Diagenetic history of Lower Palaeozoic sediments in Pomerania (northern Poland), traced across the Teisseyre–Tornquist tectonic zone using mixed– layer illite– smectite." Clay Minerals 36, no. 1 (March 2001): 15–27. http://dx.doi.org/10.1180/000985501547321.

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AbstractMixed-layer illite-smectite from Lower Palaeozoic sedimentary rocks, on both sides of the Teisseyre–Tornquist tectonic zone (TTZ) in northern Poland, was studied by X-ray diffraction and dated by K-Ar means.The percentage of smectite layers in illite-smectite (%S) indicates maximum palaeotemperatures of 125–135°C at the surface of Lower Palaeozoic rocks on the craton (NE of TTZ), and 110 to ≤180°C in different tectonic blocks to the SW of TTZ (area of Caledonian consolidation). The vertical changes in the %S indicate that the maximum palaeotemperatures were reached before Permian time on the craton, and before Jurassic, Triassic, Permian or Carboniferous periods but after the beginning of Devonian time in the Caledonian zone. The K—Ar ages of bentonites indicate that the maximum palaeotemperatures were reached by 370—390 Ma or even slightly earlier (Middle—late Devonian). A maximum of 3—6 km of Silurian–Devonian cover on the craton and in the TTZ is suggested by the data.

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25

Smaga, Łukasz, and Hidetoshi Matsui. "A note on variable selection in functional regression via random subspace method." Statistical Methods & Applications 27, no. 3 (January 25, 2018): 455–77. http://dx.doi.org/10.1007/s10260-018-0421-7.

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Abstract Variable selection problem is one of the most important tasks in regression analysis, especially in a high-dimensional setting. In this paper, we study this problem in the context of scalar response functional regression model, which is a linear model with scalar response and functional regressors. The functional model can be represented by certain multiple linear regression model via basis expansions of functional variables. Based on this model and random subspace method of Mielniczuk and Teisseyre (Comput Stat Data Anal 71:725–742, 2014), two simple variable selection procedures for scalar response functional regression model are proposed. The final functional model is selected by using generalized information criteria. Monte Carlo simulation studies conducted and a real data example show very satisfactory performance of new variable selection methods under finite samples. Moreover, they suggest that considered procedures outperform solutions found in the literature in terms of correctly selected model, false discovery rate control and prediction error.

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26

Obst, Karsten, Gerhard Katzung, Jörg Maletz, and Antje Böhnke. "Pb-Pb zircon dating of tuff horizons inthe Cyrtograptus Shale (Wenlock, Silurian) of Bornholm." Bulletin of the Geological Society of Denmark 49 (December 31, 2002): 1–8. http://dx.doi.org/10.37570/bgsd-2003-49-01.

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Waterlain fallout ashes are interbedded in the upper part of the Cyrtograptus Shale of Bornholm, theyoungest preserved member of the Lower Palaeozoic sequence at the southern coast of the island.Graptolite faunas indicate that these tuffaceous sediments belong to the Cyrtograptus lundgreni Zonedeposited during Late Wenlock. A 207Pb/206Pb mean age of 430 ± 1.9 Ma obtained by evaporation of idiomorphic single zircons from the tuff layers supports this observation. Geochemical studies of the pyroclastic rocks point to an explosive, calc-alkaline magmatic arc volcanism which probably occurred along or slightly south of the Tornquist-Teisseyre Lineament, and could have been induced by the collision of Avalonia with the southern margin of Baltica during the Silurian. This assumption is supported by the contemporaneous deposition of bentonites on the Swedish island of Gotland which might represent a distal facies of these fallouts. Further, the subduction-related volcanic activity is interpreted as a fingerprint for closing of the Tornquist Ocean during the Caledonian orogeny.

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27

Narkiewicz, Marek, and Zdzisław Petecki. "Comment on “Is the Teisseyre-Tornquist Zone an ancient plate boundary of Baltica?” by Mazur et al." Tectonics 35, no. 6 (June 2016): 1595–99. http://dx.doi.org/10.1002/2016tc004127.

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28

Vecsey, L., J. Plomerová, V. Babuška, and PASSEQ Working Group. "Mantle lithosphere transition from the East European Craton to the Variscan Bohemian Massif imaged by shear-wave splitting." Solid Earth Discussions 6, no. 1 (January 17, 2014): 229–64. http://dx.doi.org/10.5194/sed-6-229-2014.

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Abstract. We analyse splitting of teleseismic shear-wave recorded during the PASSEQ passive experiment (2006–2008) focussed on the upper mantle structure across the Trans-European Suture Zone (TESZ). 1009 pairs of the delay times of the slow split-shear waves and orientations of the polarized fast-shear waves exhibit lateral variations across the array, as well as backazimuth dependences of measurements at individual stations. While a distinct regionalization of the splitting parameters exists in the Phanerozoic part of Europe, a correlation with the large-scale tectonics around the TESZ and in the East European Craton (EEC) is less evident. No general and abrupt change in the splitting parameters (anisotropic structure) can be related to the Teisseyre–Tornquist Zone (TTZ), marking the edge of the Precambrian province on the surface. Instead, regional variations of anisotropic structure were found along the TESZ/TTZ. We suggest a south-westward continuation of the Precambrian mantle lithosphere beneath the TESZ and the adjacent Phanerozoic part of Europe, probably as far as towards the Bohemian Massif.

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29

Krzywiec, P., Ł. Gągała, S. Mazur, Ł. Słonka, M. Kufrasa, M. Malinowski, K. Pietsch, and J. Golonka. "Variscan deformation along the Teisseyre-Tornquist Zone in SE Poland: Thick-skinned structural inheritance or thin-skinned thrusting?" Tectonophysics 718 (October 2017): 83–91. http://dx.doi.org/10.1016/j.tecto.2017.06.008.

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30

Nolet, Guust, and Alet Zielhuis. "Low S velocities under the Tornquist-Teisseyre zone: Evidence for water injection into the transition zone by subduction." Journal of Geophysical Research 99, B8 (1994): 15813. http://dx.doi.org/10.1029/94jb00083.

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31

Lyskova, Eugenia, and Konstantin Sannikov. "On the anisotropy of seismic waves in the Carpathian region." E3S Web of Conferences 196 (2020): 02021. http://dx.doi.org/10.1051/e3sconf/202019602021.

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The anisotropy of seismic waves in the continental regions still belongs to the category of controversial issues, since its estimates in different areas show a different sign of the anisotropy coefficient. In contrast to studies of oceanic regions, where SH velocities always prevail over SV velocities, in the continental regions the relations between the velocities are very different. The explanation for this, first of all, is the difference in structure. The structure of the crust and upper mantle under the oceans is much more homogeneous in comparison with the structure of the continental regions. There are several approaches to the estimation of anisotropy. The most traditional method is to use the maximum amount of data separately for Love and Rayleigh waves to study the lateral distributions of SH- and SV-wave velocity, despite the fact that the density of the coverage by paths, and, consequently, the regions of best resolution can be of different shapes and sizes. It was decided to use this method as the first approximation in creating an anisotropic portrait of the Carpathian region. The Carpathian region was chosen as the object of study, since it contains interesting contrasting features: (1) the Pannonian Basin, which is characterized by a thin crust, a thinned lithosphere, and anomalously high values of the heat flux; (2) the Tornquist-Teisseyre zone, which is parallel to the strike of the Eastern Carpathians, and represents the contact zone of the Precambrian lithosphere of the EEP and the relatively young lithosphere of Western Europe. (3) The third feature is the Vrancea zone, one of the most active seismic zones in Europe. It is located in the junction of young tectonic structures: the Southern and Eastern Carpathians, the Transylvanian Depression and the Pre-Carpathian Depression. The results of the study confirm that the Tornquist-Teisseyre Zone divides the structures of the ancient East European Platform and orogenic zones of Western Europe: the upper mantle throughout EEP is characterized by high velocities, whereas velocities throughout WE are markedly lower. Low velocity anomalies prevail under Pannonian Basin which is characterized by anomalously high heat flow values. The distribution of the anisotropy coefficient demonstrates an extended layer of low values of the anisotropy coefficient at depths of 150-200 km. Above this layer, velocity distributions reveal the block structure of the lithosphere. The earthquake sources in the Vrancea zone fall into the transition zone from the highvelocity mantle under the EEP to the low-velocity mantle under the WE. Earthquakes do not occur below the revealed asthenospheric layer.

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32

Krzywiec, Piotr. "Devonian–Cretaceous repeated subsidence and uplift along the Teisseyre–Tornquist zone in SE Poland — Insight from seismic data interpretation." Tectonophysics 475, no. 1 (September 2009): 142–59. http://dx.doi.org/10.1016/j.tecto.2008.11.020.

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33

Narkiewicz, M., A. Maksym, M. Malinowski, M. Grad, A. Guterch, Z. Petecki, J. Probulski, et al. "Transcurrent nature of the Teisseyre–Tornquist Zone in Central Europe: results of the POLCRUST-01 deep reflection seismic profile." International Journal of Earth Sciences 104, no. 3 (December 10, 2014): 775–96. http://dx.doi.org/10.1007/s00531-014-1116-4.

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34

Mikołajczak, Mateusz, Stanisław Mazur, and Łukasz Gągała. "Depth-to-basement for the East European Craton and Teisseyre-Tornquist Zone in Poland based on potential field data." International Journal of Earth Sciences 108, no. 2 (December 19, 2018): 547–67. http://dx.doi.org/10.1007/s00531-018-1668-9.

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35

NARKIEWICZ, M., M. GRAD, A. GUTERCH, and T. JANIK. "Crustal seismic velocity structure of southern Poland: preserved memory of a pre-Devonian terrane accretion at the East European Platform margin." Geological Magazine 148, no. 2 (June 28, 2010): 191–210. http://dx.doi.org/10.1017/s001675681000049x.

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AbstractThe updated geological and potential fields data on the East European Platform margin in SE Poland confirm the existence of several regional units differing in Ediacaran to Silurian development: the Upper Silesian Block, Małopolska Block and Łysogóry Block. All the blocks are characterized by a distinct crustal structure seen in Vp velocity models obtained from the seismic refraction data of the CELEBRATION 2000 Programme. The first two units are interpreted as exotic terranes initially derived from Avalonia-type crust and ultimately accreted before the late Early Devonian. The Łysogóry Block is probably a proximal terrane displaced dextrally along the Baltica margin. The sutures between the terranes do not precisely match lateral gradients in Vp models. This is partly explained by a limited resolution of refraction seismic data (20 km wide interpretative window). Most of the difference is related, however, to a post-accretionary tectonism, mainly Variscan transtension–transpression. The latter processes took advantage of lithospheric memory recorded earlier as zones of rheological weakness along the former suture zones. The course of the East European Platform margin (= Teisseyre–Tornquist Zone) corresponds most likely to the Nowe Miasto–Zawichost Fault marking the NE boundary of the proximal Łysogóry Terrane.

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36

Hippolyte, J. C. "Geodynamics of Dobrogea (Romania): new constraints on the evolution of the Tornquist–Teisseyre Line, the Black Sea and the Carpathians." Tectonophysics 357, no. 1-4 (November 2002): 33–53. http://dx.doi.org/10.1016/s0040-1951(02)00361-x.

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Mazur, Stanislaw, Mateusz Mikolajczak, Piotr Krzywiec, Michal Malinowski, Vinton Buffenmyer, and Marek Lewandowski. "Reply to Comment by M. Narkiewicz and Z. Petecki on “Is the Teisseyre-Tornquist Zone an ancient plate boundary of Baltica?”." Tectonics 35, no. 6 (June 2016): 1600–1607. http://dx.doi.org/10.1002/2016tc004162.

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Guterch, A., M. Grad, R. Materzok, and E. Perchuć. "Deep structure of the Earth's crust in the contact zone of the Palaeozoic and Precambrian Platforms in Poland (Tornquist-Teisseyre zone)." Tectonophysics 128, no. 3-4 (September 1986): 251–79. http://dx.doi.org/10.1016/0040-1951(86)90296-9.

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Cole, G. A. C. "Constitution of the Earth's Interior: Volume 1 of Physics and Evolution of the Earth's Interior (Roman Teisseyre, series ed.) J. Leliwa-Kopyety ski and R. Teisseyre (eds), Elsevier, New York, 1983 368 pp., $83.00 (USA and Canada); Dfl. 195.00 (rest of world), ISBN 0 444 99646 X." Geophysical Journal International 86, no. 1 (July 1, 1986): 220–21. http://dx.doi.org/10.1111/j.1365-246x.1986.tb01088.x.

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Narkiewicz, Marek. "Comment on “Depth-to-basement for the East European Craton and Teisseyre–Tornquist Zone in Poland based on potential field data” by Mikołajczak et al." International Journal of Earth Sciences 108, no. 5 (June 12, 2019): 1763–65. http://dx.doi.org/10.1007/s00531-019-01725-7.

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Syvyi, Myroslav. "STRUCTURAL FEATURES OF THE SOUTH-WESTERN EDGE OF THE EAST- EUROPEAN PLATFORM IN THE CONTEXT OF INTERWAR RESEARCH (1918-1939)." SCIENTIFIC ISSUES OF TERNOPIL VOLODYMYR HNATIUK NATIONAL PEDAGOGICAL UNIVERSITY. SERIES: GEOGRAPHY 50, no. 1 (July 1, 2021): 14–21. http://dx.doi.org/10.25128/2519-4577.21.1.2.

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During the Polish occupation between the First and Second World Wars, scientific and exploration work in Western Ukraine was carried out by Polish, Ukrainian, Czech and Hungarian researchers. The Carpathian folded region, the Precarpathian boundary deflection, the Transcarpathian inner deflection and the Volyn-Podillia outskirts of the East European platform were studied. The main areas of research were the Carpathians and Precarpathians in connection with the discovery and development of deposits of liquid and gaseous hydrocarbons discovered here, which attracted the attention of researchers for obvious reasons. The main research conducted during this period was organized by the Geological Institute (Warsaw) and the Carpathian Geological Institute (Boryslav). No special studies have been conducted to study the structure of the Volyn-Podillia part of the East European platform at that time. After thorough work of Laskarev V.D. in 1904-1914, works which dealt mainly with local issues of tectonics appeared. This, however, significantly supplemented the existing ideas about the structural features of the region. A brief overview of studies of the structural features of the East European platform southwestern margin allows us to state the following. The most significant achievements in studying the structure of the described region were noted by such researchers as W. Teisseyre, V. Zykh, G. Teisseyre, Z. Pazdro, S. Nazarevych and others. Thus, as early as 1922 famous Polish tectonist Wawrzyniec Teisseyre proposed to consider the Holohory-Kremenets anticlinal and the Holohory flexure as independent units. They are associated with the migration of the geosynclinal axis of the Carpathians, ie with the division of the Carpathian chain into three rings (meso-, eo- and neo-Carpathians). By studying the tectonics of the foothills, he also singled out the chronological phases of migration. Comparative studies have revealed cycles of development of Precarpathian dislocations in the foothills. The initial stage of flexure development is a flat roof-like elevation preserved on the Podillia plate, with the Holohory-Kremenets anticlinal on the edge. The processes of change and disintegration of such anticlinales cause the formation of later Holohory flexures and extensive deflections. Developing his views on the decisive role of the foundation in the structure of mountain ranges and the important role of tectonic dislocations (flexures, discharges) in the nature of platform tectonics, he emphasized that transverse dislocations are the manifestation of displacements in the deep base. Russian tectonist M. Tetyaev suggested that the structure of the Transcarpathian territory is determined primarily by the folded zone of hercinide, which limits it from the west. According to him, the East European platform near the Carpathians is broken by discharges and partially hidden under the structures of the alpine fold. Ye. Oppokov, who studied the geological structure of the Devonian Podillia (Polissia) shaft, comes to the conclusion about its tectonic nature (anticlinal fold). A. Zirgoffer had a different opinion. According to the study of the relief, he believed that the Podillia shaft is a kind of barrier between the Volyn Plain and the Podillia Upland and was formed due to erosion processes. In 1928, S. Nazarevych suggested the influence of folding on the occurrence of rupture in Transnistria. According to the author the folding of gypsum, fracture of rocks of different ages (from Silurian to Neogene inclusive), the direction of the Dniester, coinciding with the main cracks, the shape of cracks may be the evidence of vigorous movements of the earth's crust, which may be the result of those mountain-building processes, which reached the maximum stress in the third age and formed Carpathians in the West. W.Teisseyre considers the fundamental issues of epeirotectonics. Based on the study of extensive Polish and foreign literature, he concludes that the network of epeirogenic lines does not correspond to the arcs of mountain ranges, and vice versa - the arcs enter at the intersection of different ages. The author opposes the understanding of epeirogenesis in the form of giant sea waves. W.Teisseyre believed that Podillia is one of the main nodes of the mountain movements of Eastern Europe. Within the Precarpathians, deep ridges and depressions are considered, established mainly according to geophysical data (Bibrka - Mykolayiv, Rozdil - Demnia, Kavske - Opary, Stara Sil - Zhuravno, etc.). From the point of view of oil and gas exploration, preference is given to the Precarpathian part of the Holohory-Kremenets-Boryslav line, then to the Dniester-Stryi basin and to the more ancient epeiroanticlinal line Smykivtsi-Kovalivka-Hrabivka-Maidan (“Stanislaviv Horst”). The importance of Transcarpathian anticlines in the search for oil and gas fields is emphasized. It is noted, in particular, that the uplift of Boryslav and Maidan - the main productive areas of the Carpathian oil and gas zone - coincides with the axes of the Podillia-Transcarpathian anticlines Holohory - Kremenets and Smykivtsi - Kovalivka. Some conclusions and generalizations were made by researchers in the interwar period (on the decisive role of the crystalline basement in the structure of mountain ranges, on the inheritance of ancient forms of the foundation surface and the chalk surface with modern relief, identified anticline uplifts in Paleozoic sediments and their oil and gas potential, on the coincidence of the axes of the Transcarpathian anticline uplifts and the main productive areas of the Carpathian oil and gas zone, etc.) have not lost their scientific value in our time and are confirmed by modern research. Studies in the 1920s and 1930s of the tectonic structure of the southwestern outskirts of the ancient East- European platform contributed to the formation of a reliable basis for the establishment and conduction of extensive exploration (oil and gas, coal, sulfur, salts, phosphorites, building materials, etc.) and systematic research in the postwar years. Key words: East European platform, tectonic structure, anticlinal uplifts, crystalline basement.

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Kravchuk, Yaroslav, and Vasyl Chalyk. "PRECARPATHIAN AND TRANSCARPATHIAN LANDFORM EVOLUTION IN THE PLIOCENE-PLEOSTOCENE AND AT EARLY STAGES." PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS, no. 09 (01) (September 25, 2019): 154–65. http://dx.doi.org/10.30970/gpc.2019.1.2808.

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The Sarmatian-Pannonian and Pontian-Pliocene stages are most important in the landform evolution of the Inner Precarpathians and Solotvyn basin. Due to the intense elevations in the upper Miocene, the Precarpathian Sea was pushed to the east and northeast. On the land freed from the sea, a hydrographic network was created, and rivers moved along the retreating sea in Northeast and Southeast directions. Original river valleys were of diagonal and inline outflow directions unlike modern transverse valleys. The Pontian-Pliocene is associated with the final phase of Carpathian and Precarpathian tectogenesis, and the proof is the undisturbed Pliocene denudation surface (Hofstein, 1985) or the upper denudation level (Teisseyre, 1933). The Solotvyno basin had continental regime before the Mukachevo basin had, so the Solotvyno basin got denudation and denudation-accumulative surfaces formed. These include the oldest denudation “Kichersky Level” researched by H. Alferyev (1948), which is believed to date to the early Pannonian. Younger denudation and denudation-accumulative surfaces are consistent with the Precarpathian and Transcarpathian regions. In the Precarpathian region, most authors distinguished two denudation-accumulative surfaces (terraces) – Krasna and Loyeva, and in the Transcarpathian, three – Dilotska, Boronyavska and Shardynska. In the Precarpathian region, they first identified pediments (Kravchuk, 1971), dating back to the Pliocene – early Pleistocene. Subsequently, I. Hofstein suggested that they should be dated the late Pliocene by analogy with the Transcarpathian pediments of Ye. Mazur (1963), but he did not deny that their formation continued in the Pleistocene. The prolonged weakening of the elevation in the early Pleistocene led to the predominance of lateral erosion, expansion of valley bottoms, and intense erosion of ancient terraces (denudation-accumulating surfaces). The analysis of terrace complexes in the Precarpathians and Transcarpathians makes it possible to determine the average heights of the Pliocene-Pleistocene elevations, which confirms the synchronicity of the landform evolution in these regions. Key words: denudation and denudation-accumulative surfaces; terraces; pediments; Pliocene-Pleistocene elevation; Precarpathians; Transcarpathians.

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Vecsey, L., J. Plomerová, and V. Babuška. "Mantle lithosphere transition from the East European Craton to the Variscan Bohemian Massif imaged by shear-wave splitting." Solid Earth 5, no. 2 (August 6, 2014): 779–92. http://dx.doi.org/10.5194/se-5-779-2014.

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Abstract. We analyse splitting of teleseismic shear waves recorded during the PASSEQ passive experiment (2006–2008) focused on the upper mantle structure across and around the Trans-European Suture Zone (TESZ). Altogether 1009 pairs of the delay times of the slow split shear waves and orientations of the polarized fast shear waves exhibit lateral variations across the array, as well as back-azimuth dependences of measurements at individual stations. Variable components of the splitting parameters can be associated with fabrics of the mantle lithosphere of tectonic units. In comparison with a distinct regionalization of the splitting parameters in the Phanerozoic part of Europe that particularly in the Bohemian Massif (BM) correlate with the large-scale tectonics, variations of anisotropic parameters around the TESZ and in the East European Craton (EEC) are smooth and of a transitional character. No general and abrupt change in the splitting parameters (anisotropic structure) can be related to the Teisseyre–Tornquist Zone (TTZ), marking the edge of the Precambrian province on the surface. Instead, regional variations of anisotropic structure were found along the TESZ/TTZ. The coherence of anisotropic signals evaluated beneath the northern part of the Brunovistulian in the eastern rim of the BM and the pattern continuation to the NE towards the TTZ, support the idea of a common origin of the lithosphere micro-plates, most probably related to Baltica. Smooth changes in polarizations of the core-mantle boundary refracted shear waves (SKS), polarizations, or even a large number of null splits northward of the BM and further across the TESZ towards the EEC indicate less coherent fabrics and a transitional character of structural changes in the mantle beneath the surface trace of the TESZ/TTZ. The narrow and near-vertical TTZ in the crust does not seem to have a steep continuation in the mantle lithosphere. The mantle part of the TESZ, whose crust was formed by an assemblage of suspect terranes adjoining the EEC edge from the southwest, appears in our measurements of anisotropy as a relatively broad transitional zone in between the two lithospheric segments of different ages. We suggest a southwestward continuation of the Precambrian mantle lithosphere beneath the TESZ and the adjacent Phanerozoic part of Europe, probably as far as towards the Bohemian Massif.

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Siwek, Grzegorz Marcin. "Charakterystyka wezbrania opadowego w zlewni górnego Wieprza w maju 2014 roku." Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia 71, no. 1 (March 6, 2017): 45. http://dx.doi.org/10.17951/b.2016.71.1.45.

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<p>Wyżyna Lubelska jest regionem, w którym co kilka lat pojawiają się intensywne opady burzowe powodujące lokalne wezbrania rzek. Szczególnie często zjawiska te pojawiają się w okolicy Krasnegostawu (Ziemnicki 1956, Dębski 1958, Maruszczak, Trembaczowski 1958, Ciepielowski, Dąbkowski 1967, Ciepielowski, Dąbkowski 1968, Górniak 1982, Kaszewski, Siwek 2005, Siwek 2010).</p><p>W świetle dotychczasowych badań (Parczewski 1960, Górniak 1982, Michalczyk 1984, Rodzik 1984, Michalczyk i in. 2008) na Wyżynie Lubelskiej katastrofalne w skutkach są ulewy o średnim natężeniu przekraczającym 1 mm∙min<sup>-1</sup>, a sumie opadu wynoszącej około 100 mm (Teisseyre 1994). Z obliczeń wynika, że prawdopodobieństwo wystąpienia opadów o tej wysokości wynosi około 1% (Suligowski 2004). W latach 1951–2000 zostało odnotowanych na Lubelszczyźnie jedynie 11 opadów o sumie dobowej >100 mm, z czego większość z nich (8 przypadków) w obszarze wyżynnym (Michalczyk i in. 2008, Siwek 2010). Kilka lat wcześniej, w międzyrzeczu Bystrzycy i Giełczwi, opad o wysokości powyżej100 mm wystąpił w nocy z 3 na 4 sierpnia 2005 roku (Michalczyk i in. 2008). Można domniemać, że najprawdopodobniej nie wszystkie epizody opadowe o sumie przekraczającej100 mm i znacznym natężeniu zostały zarejestrowane (Siwek 2006). Często o ich wystąpieniu można było wnioskować tylko na podstawie wysokiego spływu wody lub skutków geomofrologicznych. Przykładem tego są katastrofalne skutki opadów o znacznie niższych zmierzonych sumach (Maruszczak i Trembaczowski 1956, Ziemnicki 1956, Dębski 1958, Ciepielowski i Dąbkowski 1967, Ciepielowski i Dąbkowski 1968, Ciepielowski 1970, Buraczyński i Wojtanowicz 1974, Górniak 1982, Janicki i in. 2010).</p><p>Celem niniejszego opracowania jest analiza warunków powstania oraz charakterystyka hydrologiczna wezbrania w zlewni górnego Wieprza, które zarejestrowano w maju 2014 roku. W dniach 11-17 maja 2014 roku na pograniczu Wyżyny Lubelskiej i Roztocza wystąpiły opady o dużej intensywności. Stacje meteorologiczne położone na tym obszarze zarejestrowały sumy opadów sięgające od 95 do226 mm. Opad o największej intensywności wystąpił w nocy z 16 na 17 maja, kiedy to w ciągu około 3 godzin w stacji Nielisz zanotowano aż110,7 mm. W krótkim czasie nastąpiło znaczne podniesienie stanów wody w rzekach, co spowodowało ogłoszenie w kilku gminach alarmów przeciwpowodziowych (m.in. w gminie Krasnystaw). Intensywny spływ wody wywołał gwałtowne wezbranie, które spowodowało wysokie straty zarówno materialne, jak i przyrodnicze. Woda zalała ponad 2,5 tys. ha upraw, wyrządziła szkody w inwentarzu, zniszczyła dziesiątki budynków oraz odcinek drogi Zamość – Hrubieszów.</p>

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Mikołajczak, Mateusz, Stanislaw Mazur, and Łukasz Gągała. "Reply to Comment by M. Narkiewicz on “Depth-to-basement for the East European craton and Teisseyre-Tornquist Zone in Poland based on potential field data, by Mikołajczak et al., International Journal of Earth Sciences (2019) 108:547–567”." International Journal of Earth Sciences 108, no. 5 (June 12, 2019): 1767–71. http://dx.doi.org/10.1007/s00531-019-01726-6.

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Kravchuk, Yaroslav, and Yuriy Zinko. "STEPAN RUDNITSKY'S STUDIES OF THE PODILLYA RELIEF: ITS MORPHOLOGY, GENESIS AND HISTORY OF DEVELOPMENT." PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS, no. 09 (01) (September 25, 2019): 3–20. http://dx.doi.org/10.30970/gpc.2019.1.2796.

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S. Rudnitsky’s research continued in Podillya; he went on studying the morphology of genesis and history of the relief of the Carpathian and pre-Carpathian Dniester basins. Many years of expeditionary research (1903-1912) resulted in the monograph “Prerequisites for Studying Morphology of the Podilsky Catchment Area of the Dniester”, which was recommended for publication at the meeting of the Mathematical & Nature Descriptive section of the Shevchenko Scientific society (NTSh) on April 17, 1912. This work provides detailed morphographic and morphometric characteristics of the Galician Podillya relief. The monograph also reports on the formation of the Dniester basin river system, geological structure, paleogeomorphology, as well as morphological & genetic problems. In studying the Podilsky Dniester Basin, S. Rudnytsky made numerous conclusions on the problems of morphological regionalization, the relief history, in particular the formation of the Dniester valley and its Podilsky tributaries, which have not lost their relevance to this day. We can distinguish the following major points among the main findings of S. Rudnitsky's research of morphogenesis and the evolution of the Podilsky Dniester basin relief: (1) Geomorphological division of the Galician Podillya with districts allocation: Roztochya, Vereshchytsky-Shchyrets lowland, Mykolayiv-Bobretskyi “horbovyna” (land surface with hills) (Pidopillya), Opilsky “horbovyna”, Podnistriya, Podillya and Gogoloro-Kremenetsk Ridge; (2) Clarification of the history of individual regions development: the erratic Scandinavian material in Roztochya is mixed (Scandinavian-Carpathian); it is deposited by fluvia-glacial flows and represented up to altitudes of 380 m; (3) In the periglacial Pleistocene period, almost all the sands of the main areas had eolian processes; (4) Confirmation of the Podillya geological division into western and eastern with five morphological bands, proposed by W. Teisseyre; (5) Justification of the morphotectonic scheme of Podillya development, connected with tectonic elevations of the Hologoro-Kremenets Ridge, which caused the current inclination of the Podolsk hills to Southeast-East; (6) Statement that the tectonic lines of Berdo-Nârul and Kovalivka-Smykivtsi characterize the Paleozoic Platform of Podillya as a typical tectonic horst; (7) Detailed description of the Dniester “rinyshcha” (alluvial deposits) with the Carpathian material present in Podniester, Opil and Podillya itself, which are present as a strip at a distance of 14-20 km from the modern Dniester river bed; (8) Based on literary sources and his own research, the scientist came to the conclusion that there is “eolian” loess in the “rinyshcha”, sands and alluvial clay; (9) It is argued that the old Nadnistryan rivers cannot be older than the planation surfaces of the Carpathians and Pre-Carpathians; (10) Formation of the Dniester valley pattern in Pliocene and Pleistocene, which determined the direction of the flows of the left tributaries and their capture by the Western (Zakhidny) Bug river sources. Finally, in his “Prerequisites for Studying Morphology of the Podilsky Catchment Area of the Dniester” S. Rudnitsky managed to use a complex morphogenetic approach to studying the region relief for the first time geomorphological literature: from standardized morphological descriptions through systematization of the morphological structure of the region to the historical genetic interpretation of the main features of relief morphology. Key words: morphological districts; Dniester catchment area (basin); Naddnistriansky “rinyshcha” (alluvial deposits); glacial erratic material; fluvia-glacial deposits; free and entrenched meanders; “horbovyna” (land surface with hills); Podillya.

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Sim, L. A., A. V. Marinin, G. V. Bryantseva, and N. A. Gordeev. "Results of the tectonic stress study of the Northern Eurasia regions." Geodynamics & Tectonophysics 9, no. 3 (October 9, 2018): 771–800. http://dx.doi.org/10.5800/gt-2018-9-3-0371.

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The article presents the results obtained by field tectonophysical methods applied to study tectonic stresses of the Northern Eurasia regions, including young and ancient platforms (West European, Timan–Pechora, Turan, West Siberian, East European, and East Siberian) and orogenic frame structures (Caucasus, Northern Tien Shan, Mongolia-Okhotsk system of mesozoids, and Sakhalin Island). Tectonic stress reconstructions provided the basis for analysing the influence of spreading in the North Atlantics and the Arctic on the stress state of the platforms in Northern Europe. A spatial boundary of the influence goes approximately along the margins of the Fennoscandian shield and the Russian plate in the north. Further southwards, the boundary is submeridional and extends from the western wing of the Byelorussian anteclise almost to the Eastern Carpathians. The stress reconstructions for this boundary show the WNW and W-E-trending axes of compression. The boundary line does not coincide with the Teisser-Tornquist line that represents the boundary between the platforms with heterochronous basements. However, it correlates well with heat flow anomalies. The boundary area is confined to the Baltic coast [Sim, 2000. Along the boundary area, near the Baltic Sea, there is an area wherein faulting is mainly caused by extension [Sim, 2000. In this setting, helium permeability is the highest, as shown by the crust map of the European part of the USSR [Eremeev,1983. Extension in this area is probably related to formation of young grabens in the Baltic shield. Changes in the compression axis orientation may be due to the alternating activations of the grabens in the submeridionalBotnicGulf and the latitudinalGulf of Finland. Reconstructions for individual faults show contradictions in the directions of shear displacements: both right- and left-lateral displacements are possible on the same fault segments, and the axes of compression can have either latitudinal or meridional orientations. The focal mechanisms of the Osmussaar andKaliningrad earthquakes (meridional and latitudinal axes of compression, respectively) give evidence of specific current neotectonic stresses in this area. Another zone is distinguished at 52°N from the above-described area. It is mainly sublatitudinal and detected along the southern flank of the Byelorussian anteclise. Further to the east, its orientation changes to SSW, and it roughly follows the SW boundary of theVoronezh anteclise. Reconstructions for the Ukrainian Shield, located south of this zone, show mainly the unstable orientations of the axes of compression. For the platforms inNorthern Eurasia, the tectonophysical methods reconstructed neotectonic stresses in the structures formed under the influence of intraplatform tectonic stresses. These are the residual gravitational horizontal compression stresses released by long-term denudation and uplifting of the structures, including the Khibiny massif of the Baltic Shield, theOlenek and Munsky massifs of the East Siberian platform. These structures are composed of the ancient Archaean-Proterozoic rock complexes, which have been subjected to predominantly vertical displacements for a long time, from the Paleozoic to the modern stage. Special attention should be given to the tectonic stresses ofSakhalin located at the boundary between the Eurasian and North American lithospheric plates. At the edges of these two largest plates, there are the Amur and Okhotsk microplates separated by theCentral Sakhalin fault, as described in some publications. Neotectonic stress reconstructions forSakhalinIsland show sublatitudinal compression and submeridional extension in the common stress field of shearing. The tectonophysical studies show that the neotectonic stresses differ in large structures: horizontal compression and shearing are typical of the uplifts (Kola Peninsula, Tien Shan, Sakhalin), while horizontal extension and extension with shearing are characteristic of depressions (Kandalaksha graben, depressions of theTatarGulf and theSea ofOkhotsk). Our studies provide the data on spacious ‘white spots’ in the modern stress maps ofNorthern Eurasia. The stress reconstructions for practically all the studied structures show that shearing is the dominant geodynamic regime in the study region.

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"Hepato-portal and systemic hemodynamic variations in rabbit septic shock model C. Pastor, B. Teisseire and D. Payen. Laboratory of Anesthesiology, Lariboisi�re University Hospital, 2 rue Ambroise Par�, 75010 Paris, France." Journal of Molecular and Cellular Cardiology 23 (June 1991): S47. http://dx.doi.org/10.1016/0022-2828(91)90363-q.

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"L-Arginine pretreatment delays and reduces cardiovascular and hepatic hemodynamic responses to endotoxin in anesthetized rabbits C. Pastor, B. Teisseire and D. Payen. Laboratory of Anesthesiology, Lariboisi�re University Hospital, 2 rue Ambroise Par�, 75010 Paris, France." Journal of Molecular and Cellular Cardiology 23 (June 1991): S47. http://dx.doi.org/10.1016/0022-2828(91)90364-r.

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Genise, Jorge F., Juan L. Farina, and Mariano Verde. "Teisseirei barattiniaRoselli : the first sphinx moth trace fossil from palaeosols, and its distinct type of wall." Lethaia, July 2013, n/a. http://dx.doi.org/10.1111/let.12025.

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